{"title":"将大地水准面纳入澳大利亚大地测量数据还原为地心基准面的重要性","authors":"W. Featherstone","doi":"10.1080/00050342.1997.10558665","DOIUrl":null,"url":null,"abstract":"Abstract The complete reduction of terrestrial survey data to the Geodetic Reference System 1980 spheroid will become an important consideration after the implementation of the Geocentric Datum of Australia. Three examples are used to illustrate that when data reduction, which incorporates the effects of the Earth’s gravity field, is not applied, errors of approximately 10ppm, 200m and 3” can be introduced into terrain distances, astrogeodetic coordinates and azimuths respectively.","PeriodicalId":222452,"journal":{"name":"The Australian Surveyor","volume":"2022 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1997-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"22","resultStr":"{\"title\":\"The importance of including the Geoid in Terrestrial Survey Data Reduction to the Geocentric Datum of Australia\",\"authors\":\"W. Featherstone\",\"doi\":\"10.1080/00050342.1997.10558665\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract The complete reduction of terrestrial survey data to the Geodetic Reference System 1980 spheroid will become an important consideration after the implementation of the Geocentric Datum of Australia. Three examples are used to illustrate that when data reduction, which incorporates the effects of the Earth’s gravity field, is not applied, errors of approximately 10ppm, 200m and 3” can be introduced into terrain distances, astrogeodetic coordinates and azimuths respectively.\",\"PeriodicalId\":222452,\"journal\":{\"name\":\"The Australian Surveyor\",\"volume\":\"2022 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1997-03-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"22\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The Australian Surveyor\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1080/00050342.1997.10558665\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Australian Surveyor","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/00050342.1997.10558665","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The importance of including the Geoid in Terrestrial Survey Data Reduction to the Geocentric Datum of Australia
Abstract The complete reduction of terrestrial survey data to the Geodetic Reference System 1980 spheroid will become an important consideration after the implementation of the Geocentric Datum of Australia. Three examples are used to illustrate that when data reduction, which incorporates the effects of the Earth’s gravity field, is not applied, errors of approximately 10ppm, 200m and 3” can be introduced into terrain distances, astrogeodetic coordinates and azimuths respectively.
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